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By David H. Elliot

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Published by means of the yankee Geophysical Union as a part of the Antarctic study Series.

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10 ... 70 coked ... barren ... coked ... 91 52 CONTRIBUTIONS TO ANTARCTIC RESEARCH II TABLE 5.

Exposuresfrom the Nimrod Glacierto the PensacolaMountainscontain thick upper Paleozoic and Mesozoicsedimentarysequences that overlie a Copyright1991by the AmericanGeophysical Union. Precambrian and lower Paleozoicbasementcomplex of plutonic, metamorphic,and metavolcanicrocks. The continuityof this succession hasbeen attributed to developmentalongan evolvingforelandbasin[Collinson, 1990]. )-Permian diamict- 34 CONTRIBUTIONS TO ANTARCTIC ires, shales, siltstones,and sandstones[Elliot, 1975]. Continuedsubsidence preserved2500 m of Permian and Triassic rocks in the Beardmore Glacier area; theserocksweresubsequently exposedby uplift of the present-dayTransantarcticMountains.

D. d. d. d. d. d. d. d. d. 61 A1 FAURE AND BUCHANAN: ABLATION RATES OF THE ICE FIELDS NEAR ALLAN HILLS TABLE A1. (continued) TABLE A1. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. d. 800 N, 300 E (line B, Fig. 23 B1 B1 lost B1 B1 1600 S, 400 E (line C, Fig. d. d. d. d. d. d. d. d. d. 03 RecklingMoraine (Figure3) 0 2000 W A2 A1 B1 A1 A1 A2 A2 A2 Code -1 1800 N, 300 W (line A, Fig. 53 B1 B1 B1 B1 B1 B1 30 CONTRIBUTIONS TO ANTARCTIC RESEARCH TABLE A1.

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